Scattered power from non-thermal, F-region plasma observed by EISCAT - Evidence for coherent echoes?

Physics

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Coherent Scattering, Eiscat Radar System (Europe), F Region, Plasma Dynamics, Radar Echoes, Incoherent Scattering, Ion Temperature, Ionospheric F-Scatter Propagation, Monte Carlo Method, Polar Regions

Scientific paper

Three rapid, poleward bursts of plasma flow observed by the UK Polar EISCAT experiment are studied. The large ion velocities (greater than 1 km/s) are shown to drive the ion velocity distribution into non-Maxwellian form. The total scattered power is shown to rise with apparent ion temperature by up to 6 dB more than is expected for an isotropic Maxwellian plasma of constant density and by an even larger factor than expected for nonthermal plasma. The anomalous increases in power are observed only at altitudes below 300 km. At higher altitudes the rise in power is roughly consistent with that simulated numerically for homogeneous, anisotropic, non-Maxwellian plasma of constant density. The spectra at times of anomalously high power are found to be asymmetric, showing an enhancement near the downward Doppler-shifted ion-acoustic frequency. It is suggested that the data may be explained by some form of coherent echo contamination of the incoherent scatter spectrum.

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